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稀土元素地球化学研究为新疆准噶尔地区二叠纪后碰撞阶段的岩浆作用机理及地球动力学演化过程提供了重要证据。
The REE geochemical research has provided the important evidence for the mechanism of the Premian post-collision stage and the geodynamical evolution process.
目的是借鉴克拉通化概念和研究问题的思路对碰撞后和陆内阶段的构造岩浆作用的规律做一讨论。
The aim of this paper is to approach the rules of tectonomagmatic actions after the collision and in the intercontinental stage on the basis of the conception of the cratonization.
两类花岗岩的稀土元素地球化学特征明显不同,这与其所处的不同后碰撞构造演化阶段密切相关。
The characteristics of two types of granites are different, since A type and I type granites which formed at different stage of the post-collisional period.
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